半干旱土壤处理废水的理化变化,有无栽培

Solange Conceição Silva, Iara Brandão de Oliveira, Yvonilde Dantas Pinto Medeiros, Vital Pedro Da Silva Paz
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引用次数: 0

摘要

本研究评估了在存在或不存在该品种的情况下,半干旱土壤中生活污水经厌氧处理后理化属性的变化。该试验室设在巴西巴伊亚州多明戈斯市欧罗佛得州农村地区。分别以0%、25%、50%、75%、100%的比例对废水进行稀释和供水试验。土壤取样深度分别为0 ~ 35 cm (P1)和35 ~ 70 cm (P2),分别为有栽培的取样单元、无栽培的对照单元和未处理的取样单元(白色)。该品种为禾本科玉米(Zea mays L.),周期较短(60 ~ 120天)。在试验结束时,收获后,对照单位的Ca、P、K和OM的平均百分比比白色高出5%至66%,而在样品单位,由于品种的消耗,百分比高出4%至44%。TKN在采样单位中的贡献最小,足以供品种消耗。与对照单位相比,P1的Na、SAR、PST和EC的百分比分别高出35 ~ 113%和29 ~ 456%,表明该品种在P2中对阳离子的消耗较高;土壤阳离子交换部位离子分布的变化;以及土壤易于固化(PST增加)和盐碱化(EC增加)。因此,将处理过的家庭污水用于农业活动,虽然增加了土壤的养分,但由于土壤的碱度和盐度增加,产生了负面影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Physicochemical changes of semiarid soil submitted to treated wastewater, with and without cultivar
This work evaluated the changes in physicochemical attributes in semiarid soil submitted to domestic sewage submitted to anaerobic treatment, in the presence or absence of the cultivar. The experimental unit was set up in the rural area of Ouro Verde, municipality of São Domingos, state of Bahia, Brazil. Five treatments were tested by diluting wastewater and supply in the percentages 0 %, 25 %, 50 %, 75 %, and 100 %. Soil samples were taken at depths of 0 - 35 cm (P1), and 35 - 70 cm (P2) from the sampling units with cultivar, control units without cultivar, and the unit without treatment (white). The cultivar was of corn (Zea mays L.), of the family Poaceae, which has a relatively short cycle (60 - 120 days). At the end of the experiments, after the harvest, the control units presented average Ca, P, K, and OM percentages from 5% to 66 % higher than white, while in the sample units, the percentages were 4% to 44 % higher, due to consumption by the cultivar. The contribution of TKN in the sampling units was the minimum sufficient for consumption by the cultivar. Compared to the control units, the sampling units presented Na, SAR, PST, and EC percentages higher by 35 - 113 % in P1, and by 29 – 456 % in P2, which indicates a higher consumption of cation by the cultivar in P2; change of ion distribution in the soil cation exchange site; as well as predisposition of the soil to sodification (increase of PST) and salinization (increase of EC). Consequently, the application of treated domestic effluents for agricultural activity, although it adds nutrients to the soil, has negative effects due to the increase in soil sodicity and salinity.
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